using gps to measure precipitable water vapor in antarctica
TRANSCRIPT
GPS signal delays
• GPS is broadcast on
the L1 and L2 signals
• Precipitable Water
Vapor (PWV) can be
extracted from the
signal delay
www.redorbit.com/modules/reflib/article_images/21_aab02a40d790b5bdb771c2f0fd2fc6d0.jpgwww.trimble.com/gps/howgps-error.shtml
Atmospheric Mesoscale Prediction System
• At present, a reliable source for predictions• Predicts model data for multiple variables• Makes predictions every 6 hours
• 2-meter temperature (k)• Surface pressure (hPa)• Moisture (mm)
Map Making
• AMPS data downloaded for 2005
• Variables geocoded to 30km x 30km grid
• 4500 maps for each variable
Temperature Moisture Pressure
Interpolation – the beginningStar – GPS site
Latitude point80° south
This is a small slice of Southern
Victoria Land.
Interpolation• Latitudes for each GPS site used
• Extracted values from each variable for GPS sitesMoisture Temperature Pressure
Calculations
• ZHD = 2.2779*(Ps/(1-0.00266*COS(2λ)-0.00028*H))
• λ = latitude in radians
• H = height of GPS site above the ellipsoid in km
• Ps = surface pressure in hPa
• ZWD = ZPD - ZHD
• PW = П * ZWD
Differences (at each GPS site)
• Acquired ZPDs for 23 of 31 GPS sites
• Observations taken every 2 hours
• Each site has different number of observations
• Matched up ZPDs to variables
Problems & Solutions• Possibly using 2 different ellipsoids• Pressure values could be inaccurate• Zenith Neutral Delays could be of bad quality
• Find out if model values are on a topographical model or ellipsoidal model
• Interpolate model ‘elevations’ and compare to actual height above ellipsoid
• Use interpolated values (if correct) in ZHD equation
Importance?
• More accurate weather forecasts
• Improve current climate models
• Contribute to studies of climate change
• Further insight into any ongoing climate change in Antarctica